Editorial Feature

Tremolite - Occurrence, Properties, and Distribution

Tremolite is a member of the amphibole group of silicate minerals. It is formed by metamorphism of quartz and dolomite-rich sediments. It was first discovered in 1789 in Campolungo, Piumogna Valley in Ticino, Switzerland.

Properties of Tremolite

The following are the key properties of Tremolite:

  • Cell Data
    • Space Group: C2/m
    • a = 9.863(1)
    • b = 18.048(2)
    • c = 5.285(1)
    • β = 104.79(1)°
    • Z = 2

  • Crystal Data
    • Monoclinic
    • Point Group: 2/m
    • Elongated, stout prismatic, or flattened bladed crystals, to 20cm. Also fibrous, granular or columnar aggregates
    • Twinning: Simple or multiple, common || {100}; rarely multiple || {001}
    • X-ray powder pattern: 8.38 (100), 3.121 (100), 2.705 (90), 3.268 (75), 1.892 (50), 2.805 (45), 2.015 (45)

  • Chemical Composition
    Elements Content 1 Content 2
    SiO2 56.57 59.3
    MgO 24.41 24.58
    CaO 12.25 12.03
    F 1.52 3.84
    H2O+ 1.46 0.5
    Na2O 1.44 2.07
    Al2O3 1.41 0.26
    K2O 0.68 0.61
    -O = (F, Cl)2 [0.64] [1.62]
    FeO 0.08 trace
    Cl 0.05 trace
    MnO 0.03 trace
    TiO2 0.01 trace
    Total [99.27] [101.57]

  • Optical Properties
    • Biaxial (-)
    • Orientation: Y = b
    • Z ^ c = -21° to -19°
    • X ^ a = -6° to -4°
    • Dispersion: r < v, weak
    • α = 1.605 - 1.613
    • β = 1.616 - 1.624
    • γ = 1.630 - 1.636
    • 2V(meas.) = 86° - 88°
  • Estimated Properties
    Electron density Bulk density (electron density)=2.98 g/cm3
    note: Specific gravity of Tremolite =2.98 g/cm3
    Photoelectric PETremolite = 2.61 barns/electron
    U= PETremolite x ρElectron density= 7.76 barns/cm3
    Fermion index Fermion index = 0.02
    Boson index = 0.98
    Radioactivity
    Tremolite is not radioactive

How to Identify Tremolite

Pure tremolite can be found in brown, white, light-green, gray, or colorless forms. It has a transparent to translucent appearance with a white streak, vitreous luster, and fluorescent luminescence.

It can be observed as massive, fibrous, granular, or columnar structures, with perfect and distinct cleavages. The relative hardness of tremolite ranges from 5 to 6, and its average density is 3.05 g/cm3.

Global Distribution

Tremolite is distributed in the following places:

  • Campolungo Alp, Ticino
  • Bristenstock, Uri, Switzerland
  • St. Marcel, Piedmont, Italy
  • Bilin, Czech Republic
  • Macomb, St. Lawrence Co. New York
  • Sussex Co. New Jersey
  • Lee, Berkshire Co. Massachusetts
  • Wilberforce, Ontario, Canada
  • Kozano, Badakhshan Province, Afghanistan
  • Lelatema, Tanzania
  • Brumado mine, Bahia, Brazil

Occurrence of Tremolite and Useful Mineral Association

Tremolite occurs in greenschist facies metamorphics, derived from ultramafic or magnesium carbonate rocks.

It is closely associated with winchite, riebeckite, magnesio-cummingtonite, cummingtonite, forsterite, diopside, talc, wollastonite, calcian garnet, dolomite, and calcite.

References

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